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Astron. Astrophys. 320, L37-L40 (1997) 3. ResultsEven though GRS1915+105 was observed in the pointed-mode for 4 days
during the period July 20-29, 1996 the useful data are for about 8850
seconds due to various operational constraints. Almost all the count
rates were acquired with an integration time of 0.1 sec. The X-ray
light curve for the entire period of useful observations showed no
large scale intensity variations on time scale of a minute or longer.
This is unlike the results reported in the higher energy band
(Castro-Tirado et al. 1994 ; Sazonov et al. 1994 ). Analysis of data
on shorter time scale, however, shows pronounced variations on time
scale of a second and less. A few typical light curves showing
sub-second intensity variations are shown in figure 1. These
variations were detected independently in each detector with similar
count rate profiles. Further the veto layer count rates do not exhibit
this kind of variability. It will be noticed from the light curves
that GRS 1915+105 shows frequent flaring activity on time scales of
less than a second and occasionally over 0.1 sec. During the flares
the intensity varies by a factor of upto 3 in less than a second. From
analysis of the flare frequency in GRS1915+105 and Cyg X-1, we find
that flare occurrence in GRS1915+105 is less common than that in Cyg
X-1. Details of flaring activity in Cyg X-1 will be reported in a
separate paper (Rao et al. 1997). During the sporadic intensity
variations, the light curves of the two sources exhibit remarkable
similarity at time scale of 0.1 to 1 second. Power density spectrum
and Fast Fourier Transform (FFT) analysis showed no variability with a
fixed period indicating that the source is not an X-ray pulsar.
However, strong Quasi- Periodic Oscillation (QPOs) were detected from
GRS1915+105 in all the data. The periodogram is shown in figure 2. The
QPOs are clearly detected independently at the same frequency in the
data of each PPC as well as in the summed data. The QPO frequency
however varies in an erratic manner from day to day. A summary of the
observations and QPO characteristics is given in Table I. It will
be noticed that the QPO frequency varied from 0.62 to 0.82 Hz. The rms
fraction in QPO is typically about 10%. Besides the 0.7 Hz peak the
summed power spectrum also shows another less prominent peak at
Table 1. IXAE observations and results of GRS1915+105 Anticorrelation between the total intensity and hardness ratio (6-18 keV to 2-6 keV) is seen at very small time scale. Details of the analysis will be reported in a separate paper. ![]() ![]() ![]() ![]() © European Southern Observatory (ESO) 1997 Online publication: June 30, 1998 ![]() |